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Wyświetlanie 1-11 z 11
Tytuł:
Crystallochemical Structure of Tourmalines Inferred from Mössbauer Spectroscopy
Autorzy:
Kraczka, J.
Pieczka, A.
Powiązania:
https://bibliotekanauki.pl/articles/2028978.pdf
Data publikacji:
2001-11
Wydawca:
Polska Akademia Nauk. Instytut Fizyki PAN
Tematy:
76.80.+y
Opis:
In the Y octahedra of tourmalines theoretically may occur ions of Fe$\text{}^{2+}$ and Fe$\text{}^{3+}$. The authors discuss Mössbauer measurements and confirm the ordered model of ionic distribution at these sites: the presence of Fe$\text{}^{3+}$ ions in the Y octahedra and Al$\text{}^{3+}$ ions in the Z octahedra. The spectra of different tourmalines annealed at temperatures ranging from 873 K to 1153 K show that Fe$\text{}^{3+}$ ions can occur in both of these sites. The annealing has changed the symmetry of the neighbourhood of iron ions at the octahedral sites. It has been shown that the doublets with QS<2.00 mm/s should not been attributed to Fe$\text{}^{2+}$(Z). Also new results corroborating the existence of the iron ions in the mixed valence state in tourmalines have been presented.
Źródło:
Acta Physica Polonica A; 2001, 100, 5; 743-750
0587-4246
1898-794X
Pojawia się w:
Acta Physica Polonica A
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The Rietveld refinement of beryls from pegmatitic system at Piława Górna, Góry Sowie Block, SW Poland
Autorzy:
Zelek-Pogudz, S.
Zubko, M.
Pieczka, A.
Powiązania:
https://bibliotekanauki.pl/articles/1058118.pdf
Data publikacji:
2016-10
Wydawca:
Polska Akademia Nauk. Instytut Fizyki PAN
Tematy:
91.65.An
Opis:
The studied beryl crystals came from the Julianna pegmatitic system exposed in the Dolnośląskie Surowce Skalne S.A. quarry at Piława Górna. This mineral occurs here in various forms and colours (green, yellow, white, pinkish and blue) in almost all pegmatite bodies. The paper describes the relationship between the structure and chemical composition of different coloured beryl crystals.
Źródło:
Acta Physica Polonica A; 2016, 130, 4; 898-900
0587-4246
1898-794X
Pojawia się w:
Acta Physica Polonica A
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Ti remobilization and sulphide/sulphoarsenide mineralization in amphibolites: effect of granite intrusion (the Karkonosze–Izera Massif, SW Poland)
Autorzy:
Mochnacka, K.
Oberc-Dziedzic, T.
Mayer, W.
Pieczka, A.
Powiązania:
https://bibliotekanauki.pl/articles/2059096.pdf
Data publikacji:
2008
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Karkonosze granite
Ti mineralization
hydrothermal sulphide/sulphoarsenide mineralization
contact metamorphism
Opis:
Our studies focus on ore mineralization in a contact-metamorphic aureole, using the Variscan Karkonosze Granite pluton as an example. The Karkonosze in trusion is enveloped by an Early Palaeozoic (about 500 Ma) metamorphic complex of the Izera–Kowary Unit composed of a diverse assemblage of gneisses, granitic gneisses, schists, amphibolites and marbles. The Budniki ore mineralization site was discovered in the early 1950's at the SE margin of the pluton. The uneconomic Ti-ox ide/sil i cate, Fe-Cu-Ni-Co-sulphide-sulphoarsenide, and uranium mineral deposits are hosted within amphibolites which were subjected to regional metamor phism fol lowed by contact meta - morphism. The Ti mineralization includes an ilmenite-titanite assemblage that originated from regional-metamorphic transformation of igneous Ti-bearing minerals, such as ilmenite and tschermakite, of the basic protoliths of amphibolites. During subsequent contact metamorphism, ilmenite was decomposed and, after wards, Al-rich titanite and rutile were formed. The Ti remobilization was coeval with an early stage of superimposed Fe-Cu-Ni-Co-sulphide/sulphoarsenide mineralization (pyrrhotite, pyrite, pentlandite, arsenopyrite, chalcopyrite, sphalerite and Fe-Ni-Co-As-S phases), related to the activity of the Karkonosze Granite hydrothermal system. The ore minerals formed successively within a wide range of temperatures (625–250gradeC).
Źródło:
Geological Quarterly; 2008, 52, 4; 349-349
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Ore mineralization in the Miedzianka area (Karkonosze-Izera Massif, the Sudetes, Poland): new information
Autorzy:
Mochnacka, K.
Oberc-Dziedzic, T.
Mayer, W.
Pieczka, A.
Powiązania:
https://bibliotekanauki.pl/articles/2086527.pdf
Data publikacji:
2012
Wydawca:
Polskie Towarzystwo Mineralogiczne
Tematy:
Miedzianka
Ciechanowice
Przybkowice
Karkonosze-Izera Massif
ore deposits
mineral succession
geothermometry
Opis:
The Miedzianka mining district has been known for ages as a site of polymetallic ore deposits with copper and, later, uranium as the main commodities. Although recently uneconomic and hardly accessible, the Miedzianka ores attract Earth scientists due to the interesting and still controversial details of their ore structure, mineralogy and origin. Our examination of the ore mineralization from the Miedzianka district was based exclusively on samples collected from old mining dumps located in the vicinity of Miedzianka and Ciechanowice, and on samples from the only available outcrop in Przybkowice. In samples from the Miedzianka field, chalcopyrite, pyrite, galena, bornite, chalcocite, digenite, arsenopyrite, magnetite, sphalerite, tetrahedrite-tennantite, bornite, hematite, martite, pyrrhotite, ilmenite, cassiterite and covellite are hosted in quartz-mica schists and in coarse-grained quartz with chlorite. In the Ciechanowice field, the ore mineralization occurs mainly in strongly chloritized amphibolites occasionally intergrown with quartz and, rarely, with carbonates. Other host-rocks are quartz-chlorite schist and quartzites. Microscopic examination revealed the presence of chalcopyrite, pyrite, sphalerite, galena, tetrahedrite-tennantite, bismuthinite, native Bi, arsenopyrite, löllingite, cassiterite, cobaltite, gersdorffite, chalcocite, cassiterite, bornite, covellite, marcasite and pyrrhotite. Moreover, mawsonite and wittichenite were identified for the first time in the district. In barite veins cross-cutting the greenstones and greenschists in Przybkowice, we found previously-known chalcopyrite, chalcocite and galena. The composition of the hydrothermal fluids is suggested to evolved through a series of consecutive systems characterized, in turn, by Ti-Fe-Sn, Fe- As-S, Fe-Co-As-S, Cu-Zn-S and, finally, Cu-Pb-Sb-As-Bi compositions.
Źródło:
Mineralogia; 2012, 43, 3/4; 155--178
1899-8291
1899-8526
Pojawia się w:
Mineralogia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The philipsbornite–segnitite solid-solution series from Rędziny, eastern metamorphic cover of the Karkonosze granite (SW Poland)
Autorzy:
Gołębiowska, B.
Włodek, A.
Pieczka, A.
Borkiewicz, O.
Polak, M.
Powiązania:
https://bibliotekanauki.pl/articles/191534.pdf
Data publikacji:
2016
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
arsenates
oxidation zone
philipsbornite
segnitite
carminite
chemical composition
Rędziny
Opis:
Supergene minerals of the philipsbornite–segnitite series, PbAl3(AsO4)(AsO3OH)(OH)6–PbFe3+3(AsO4) (AsO3OH)(OH)6, accompanied by carminite, PbFe3+2(AsO4)2(OH)2, were found in relics of hydrothermal quartz– chlorite–arsenopyrite veins, associated with subordinate polymetallic ores disseminated in contact zones of a dolomitic marble deposit at Rędziny, Western Sudetes, Poland, and recognized by means of electron microprobe and X-ray and electron-back-scattered diffraction (XRD and EBSD). Philipsbornite and segnitite, as the two minerals of the series, exhibit highly variable compositions, especially in terms of the range of Fe3+ Al3+ substitution at the G site, with a distinct gap between the values of 0.52 and 0.89 for the Fe/(Al+Fe) ratio; substitutions at the D and T sites are less important. In this respect, the minerals are almost identical with philipsbornite and segnitite, known from other localities. The gap might be a consequence of the limited miscibility of the end-members, but also might be attributed to crystallization under the changing and distinctly differing activities of Al3+ and Fe3+. The unit-cell parameters of philipsbornite, a = 7.1245(13) Ο, c = 17.0967(45) Ο, make the mineral comparable with philipsbornites from other occurrences. The EBSD analysis confirmed the rhombohedral structure of both minerals and the space group symmetry R-3m. The minerals crystallized in the sequence: philipsbornite -> segnitite -> carminite, which reflects (i) decreasing acidity in the oxidation zone, due to the leaching of sulphate ions and interaction of the solutions with a nearby dolomite lens, and (ii) varying activities of Al3+, Fe3+ and Pb2+ cations, mobilized by the solutions through interaction with the silicate host containing disseminated arsenopyrite and subordinate sulphides, up to complete Pb2+ depletion.
Źródło:
Annales Societatis Geologorum Poloniae; 2016, 86, 1; 73-83
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Żelazowo-żelazawe odmiany sepiolitu i saponitu z diabazów z Niedźwiedziej Góry koło Krakowa
Ferriferrous varieties of sepiolite and saponite from the diabases of Niedźwiedzia Góra near Kraków
Autorzy:
Gaweł, A.
Muszyński, M.
Pieczka, A.
Skowroński, A.
Stoch, P.
Powiązania:
https://bibliotekanauki.pl/articles/183659.pdf
Data publikacji:
2008
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
dolnopermskie wulkanity
diabazy
żyły epitermalne
sepiolit żelazowo-żelazawy
saponit żelazowo-żelazawy
Lower Permian volcanites
diabases
epithermal veins
ferriferrous sepiolite
ferriferrous saponite
Opis:
W żyłach szczelinowych napotkanych w tzw. diabazach z Niedźwiedziej Góry koło Krakowa zidentyfikowano rzadko występujące w przyrodzie żelazowo-żelazawe odmiany sepiolitu: [wzór] i saponitu: [wzór]. Towarzyszą im: kwarc +/- chalcedon, kalcyt oraz podrzędnie - piryt, markasyt, sfaleryt, baryt, fluorowy apatyt i tlenki Ti-Fe (ilmenit?). Żyły powyższe stanowią wyraźnie wyróżniający się system, który należy wiązać z epitermalną działalnością pomagmową. Zasobny w żelazo sepiolit, minerały grupy SiO2, kalcyt, baryt oraz siarczki Fe i Zn wykrystalizowały w szczelinach bezpośrednio z roztworów. Silnie żelazisty saponit jest natomiast produktem przeobrażenia obecnego pierwotnie w szczelinach rumoszu diabazów (apatyt i tlenki Ti-Fe są reliktowo zachowanymi ich składnikami) pod wpływem tych roztworów. Saponit powstał pierwotnie zapewne jako odmiana żelazawa, w środowisku redukcyjnym. Jego aktualny, żelazowo-żelazawy charakter jest efektem późniejszego oddziaływania zasobnych w tlen wód descenzyjnych, zachodzącego po zerodowaniu nadległych skał karbonu i części sillu diabazowego.
In fracture veins found in the so-called diabases of Niedźwiedzia Góra near Cracow the authors have identified ferriferrous varieties of sepiolite: [formula] and saponite: [formula], two minerals rarely occurring in the nature. They are accompanied mainly by quartz (sometimes with chalcedony) and calcite, whereas less frequently by pyrite, marcasite, sphalerite, barite, fluorapatite and Ti-Fe oxides (ilmenite?). The veins represent a distinct system that must be interpreted as a result of epithermal postmagmatic activity. The sepiolite rich in iron, the minerals of the SiO2 group, calcite, barite and Fe and Zn sulphides crystallized directly from solutions in rock fractures. The iron-rich saponite is, in turn, a product of alteration of the diabase rubble present initially in the fractures (apatite and Ti-Fe oxides are its relicts), affected by these solutions. The saponite must have originated as a ferrous variety in a reducing environment. Its current, ferriferrous character is an effect of later changes imparted by descending, oxygen-rich waters, percolating through the fractures after the erosion removed overlaying Carboniferous rocks and an upper part of the diabase sill.
Źródło:
Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie; 2008, 34, 1; 19-42
0138-0974
Pojawia się w:
Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Isotopic Re-Os age of molybdenite from the Szklarska Poręba Huta Quarry (Karkonosze, SW Poland)
Autorzy:
Mayer, W.
Creaser, R. A.
Mochnacka, K.
Oberc-Dziedzic, T.
Pieczka, A.
Powiązania:
https://bibliotekanauki.pl/articles/2059392.pdf
Data publikacji:
2012
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Karkonosze granite
hydrothermal mineralisation
Re/Os isotopic age
Opis:
New Re/Os isotopic data for molybdenite from the Szklarska Poręba Huta Quarry provide ages of 307 ± 2 Ma and 309 ± 2 Ma, respectively. The quarry is dominated by the porphyritic (“central”) and equigranular (“ridge”) varieties of the Karkonosze granite. Ore mineralisation hosted in aplogranite includes an assemblage of sulphides, sulphosalts, oxides and various rare phases. The molybdenite ages obtained are consistent with a previously published isotopic age of leucogranite (aplogranite?) from the same quarry and are only slightly older than a recently published, refined 2 6Pb/238U age of untreated zircons from the Szklarska Poręba Huta porphyritic granite. The age of the molybdenite corresponds moderately well to the younger stage of post-magmatic, pneumatolitic/hydrothermal activity of the Karkonosze granite (about 312 Ma).
Źródło:
Geological Quarterly; 2012, 56, 3; 505--512
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Preliminary results of sulphur isotope studies on sulfides from selected ore deposits and occurrences in the Karkonosze–Izera Massif (the Sudety Mts., Poland)
Autorzy:
Mayer, W.
Jędrysek, M.O.
Górka, M.
Drzewicki, W.
Mochnacka, K.
Pieczka, A.
Powiązania:
https://bibliotekanauki.pl/articles/2086529.pdf
Data publikacji:
2012
Wydawca:
Polskie Towarzystwo Mineralogiczne
Tematy:
Karkonosze-Izera Massif
sulphur isotope studies
polymetallic mineralization
Opis:
Preliminary sulphur isotope data are presented for selected ore deposits and occurrences in the Karkonosze-Izera Massif, namely, polymetallic mineralization sites at Budniki, Ciechanowice, Izerskie Garby and Sowia Dolina, and the pyrite deposit at Wieściszowice. The data reveal two populations of δ34S values: from 2.74 to 3.95‰ (pyrrhotites and pyrites in Sowia Dolina, and some pyrites in Wieściszowice) and from 0.79 to 1.8‰ (pyrites in Budniki, Ciechanowice and Izerskie Garby, and some pyrites from Wieściszowice). All of the data are indicative of endogenic sulphur typical of hydrothermal mineralization despite the genetic differences between the sites.
Źródło:
Mineralogia; 2012, 43, 3/4; 213--222
1899-8291
1899-8526
Pojawia się w:
Mineralogia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Studies on magnetite and pyrite mineralization, and on their early Palaeozoic ocean-floor host-rocks from the Leszczyniec Unit (West Sudetes, Poland)
Autorzy:
Oberc-Dziedzic, T.
Mochnacka, K.
Mayer, W.
Pieczka, A.
Creaser, R. A.
Góralski, M.
Powiązania:
https://bibliotekanauki.pl/articles/191471.pdf
Data publikacji:
2011
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
magnetite and pyrite mineralization
metabasites
ocean-floor metamorphism
paragonite
Leszczyniec Unit
Sudetes
Polska
Opis:
The Leszczyniec Unit extends along the eastern margin of the Karkonosze-Izera Massif. It comprises the Early Palaeozoic, MORB-like Leszczyniec complex composed of metabasites, metagranites and metasedi- ments. The metabasites host magnetite mineralization encountered in Jarkowice, whereas near Wieściszowice village the pyrite deposit occurs in metasediments and metabasites. The common feature of both sites is the almost complete absence of the accompanying ore minerals. Basing on petrographic, mineralogical, geochemical and microstructural studies, it was found that the metabasic rocks, which host magnetite mineralization, were lava flows, whereas the protoliths of pyrite-bearing schists were basic and acid tuffites accompanied by ocean-floor basalts. The igneous rocks from the Leszczyniec Unit were subjected to the ocean-floor metamorphism, whereas the accompanying sediments were altered by hydrothermal fluids enriched in sulphur ions, which reacted with iron derived from the sediment and promoted crystallization of pyrite. The sources of hydrothermal fluids were adjacent magmatic centres. The estimated age ~480 Ma for pyrite (Re-Os method) is similar to the previously known ~500 Ma age of metabasites (U-Pb, zircon method) from the Leszczyniec Unit, which establishes a temporal link between pyrite accumulation and the ocean-floor environment. The rocks of the Leszczyniec Unit, first altered by the ocean-floor metamorphism and the hydrothermal fluids, were subsequently subjected to the regional metamorphism at 360–340 Ma and the two-stage deformations of various intensities, followed by the third stage of deformations which caused the reorientation of the regional foliation. The zones of ductile and brittle deformations connected with the second deformation event host the accumulations of magnetite formed at the expense of Fe-bearing rock-forming minerals or from iron supplied from adjacent sources. In the pyrite-bearing schists, mineral assemblages formed during the hydrothermal alteration have been subjected to recrystallization and were included into domains defining foliation and lineation, which formed during the first stage of deformation. Pyrite crystals were affected by both deformation stages. At the end of the second stage, the invasion of fluids led to the dissolution of pyrite crystals and to the filling of cracks in pyrite crystals with chalcopyrite and tennantite. This process was followed by the formation of quartz veins with minor amounts of ore minerals.
Źródło:
Annales Societatis Geologorum Poloniae; 2011, 81, No 2; 133-160
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The Julianna pegmatite vein system at the Piława Górna Mine, Góry Sowie Block, SW Poland – preliminary data on geology and descriptive mineralogy
Autorzy:
Szuszkiewicz, A.
Szełęg, E.
Pieczka, A.
Ilnicki, S.
Nejbert, K.
Turniak, K.
Banach, M.
Łodziński, M.
Różniak, R.
Michałowski, P.
Powiązania:
https://bibliotekanauki.pl/articles/2060610.pdf
Data publikacji:
2013
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
rare-element pegmatite
mixed (NYF + LCT) signature
granitic pegmatites
Piława Górna
Góry Sowie Block
Sudetes
Opis:
The newly discovered Julianna pegmatitic system from the Piława Górna Quarry (the Góry Sowie Block, Sudetes Mts., NE margin of the Bohemian Massif) is described in terms of geological setting, petrography and descriptive mineralogy. The system represents the largest pegmatitic occurrence in the Polish Sudetes and consists of a complex network of cogenetic rare-element granitic pegmatites that intruded into tectonized amphibolite as discordant dikes. The pegmatites range from barren and weakly zoned to texturally well-differentiated ones that are composed of a fine-grained border zone, coarse-grained wall zone, graphic and blocky feldspar intermediate zones and a quartz core. Unidirectional and skeletal solidification textures are well-developed. The Julianna pegmatites consist of rock-forming plagioclase (ŁAn39), microcline, quartz and biotite accompanied mostly by accessory to minor muscovite, tourmaline, garnet and beryl. They crystallized from anatectic melt of hybrid NYF (niobium-yttrium-fluorine) + LCT (lithium-cesium-tantalum) geochemical characteristics. Pegmatites with a low to moderate degree of fractionation, that dominate in the Julianna system, bear NYF-signature accessory minerals, such as allanite-(Ce), columbite-, euxenite- and samarskite-group minerals, fergusonite-(Y) and gadolinite-(Y). However rare dikes that attained a very high degree of fractionation contain typical minerals of LCT-signature including tourmalines of the elbaite-olenite-rossmanite series, lepidolite, lithiophilite, spodumene, Cs-rich beryl and pollucite.
Źródło:
Geological Quarterly; 2013, 57, 3; 467--484
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Znaczenie przestrzeni w procesie scalania miasta
The importance of the space in the process of merging the city
Autorzy:
Hereć, A.
Pieczka, M.
Skoczylas, O.
Powiązania:
https://bibliotekanauki.pl/articles/389966.pdf
Data publikacji:
2017
Wydawca:
Politechnika Lubelska. Wydawnictwo Politechniki Lubelskiej
Tematy:
scalanie miasta
miejsca spotkań
partycypacja społeczna
tożsamość miejsca
przestrzeń publiczna
merge the city
meeting places
social participation
identity of the place
public space
Opis:
W procesie scalania miasta integralną rolę stanowi dostrzeżenie rangi przestrzeni wspólnych jako miejsc koncentracji aktywności międzyludzkich. Potrzeba miejsc spotkań jest wynikiem natury człowieka i warunkuje jego percepcję przestrzeni. Środowisko miejskie jest głównie postrzegane przez mieszkańców przez pryzmat formy i charakteru przestrzeni wspólnych. To właśnie przestrzenie wspólne stanowią wizytówkę osiedli, dzielnic, miast tworząc poczucie przywiązania – łączności z danym miejscem. Jakość wnętrz urbanistycznych wpływa na budowanie więzi społecznych a przez to na atrakcyjność środowiska miejskiego. Nieodpowiednie dostosowanie przestrzeni publicznych dezintegruje strukturę miejską, w efekcie utrudnia, a wręcz uniemożliwia identyfikację z danym miejscem. Konfrontacja rzeczywistości z potrzebą zmian niejednokrotnie aktywizuje lokalne społeczności do działań, które przy współpracy z architektem zmieniają przestrzeń (jak w sztokholmskiej dzielnicy Tensta-Piazza Taxingeplan). Działania spajające strukturę miejską przybierają różnorodne formy, jednak najczęściej prowadzą do wytworzenia przestrzeni o charakterze dospołecznym, skłaniającej mieszkańców do integracji.
An integral part of the process of uniting the city is to notice importance of common places as fields of concentration of interpersonal acting. The need for gathering places is the result of human nature and determines space perception. The urban habitat is perceived by citizens mainly through the form and nature of the common areas. First of all common spaces showcase the settlements, neighborhoods, cities and create a sense of bond - attachment with the place. The quality of urban interiors affects the formation of social ties and thereby the attractiveness of the urban environment. Improper adjustment of public spaces disintegrates urban structure. In effect makes it difficult or even impossible to identify with the place. The confrontation of the reality with the need for change often stimulates local community to action, which change space in collaboration with the architect (as in the Stockholm district Tensta - Piazza Taxingeplan). Actions bonding urban structure can take various forms but most commonly lead to formation a space oriented to users, encouraging residents to integration.
Źródło:
Budownictwo i Architektura; 2017, 16, 1; 175-182
1899-0665
Pojawia się w:
Budownictwo i Architektura
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-11 z 11

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